Abstract

Ambient PM 10 and PM 2.5 at Puertollano (central Spain) are derived mostly from local industrial emissions (including a refinery and power stations) and mineral (“crustal”) aerosols from fugitive dusts and African intrusions. Vanadium and the lanthanoid elements (La to Lu) can be used as geochemical markers to help identify these different contributions, especially when combined with atmospheric back-trajectory data. The total lanthanoid (∑Loid) content of PM is controlled primarily by the amount of coarse crustal material present, with the highest values being recorded in PM 10 during an African dust intrusion (13 ng m −3). In contrast, La/Ce and La/Sm ratios are controlled by fine refinery emissions, rising above natural crustal averages due to the release of La from fluid catalytic converters (FCC), and allowing the identification of La anomalies (La > Ce) when FCC emissions are prominent. Crustal La/Ce ratios are least common, and La anomalies most common, in PM 2.5 measured during local pollution events. Increasing contamination of urban/industrial atmospheric PM samples away from crustal compositions may be tracked using a LaCeSm triangular plot, but this does not differentiate between FCC refinery and oil combustion emissions. Comparing lanthanoid and V concentrations does aid such differentiation, although given the likelihood of multiple PM sources in industrial locations, we recommend use of a LaCeV plot rather than simply La/V ratios.

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